Geochemical and geophysical implications of the radiocarbon calibration
- 1 June 1998
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 62 (12) , 2025-2038
- https://doi.org/10.1016/s0016-7037(98)00130-6
Abstract
No abstract availableKeywords
This publication has 77 references indexed in Scilit:
- Deep-Sea Coral Evidence for Rapid Change in Ventilation of the Deep North Atlantic 15,400 Years AgoScience, 1998
- Solar modulation of cosmogenic nuclide production over the last millennium: comparison between 14C and 10Be recordsEarth and Planetary Science Letters, 1997
- Deglacial sea-level record from Tahiti corals and the timing of global meltwater dischargeNature, 1996
- 230Th-234U and 14C Ages Obtained by Mass Spectrometry on CoralsRadiocarbon, 1993
- Increases in terrestrial carbon storage from the Last Glacial Maximum to the presentNature, 1990
- Evidence for long-term brightness changes of solar-type starsNature, 1990
- U-Th ages obtained by mass spectrometry in corals from Barbados: sea level during the past 130,000 yearsNature, 1990
- Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U–Th ages from Barbados coralsNature, 1990
- Retreat velocity of the North Atlantic polar front during the last deglaciation determined by 14C accelerator mass spectrometryNature, 1987
- 14C measurements on foraminifera of deep sea core V28-238 and their preliminary interpretationNuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 1984